Rate-and-state friction of epidote gouge under hydrothermal conditions and implications for the stability of subducting faults under greenschist metamorphic conditions

Epidote is a common hydrous mineral present in subduction zones subject to greenschist metamorphic conditions – and potentially an important control on the fault stability-instability transition observed under greenschist facies. We explore controls on this transition through shear experiments on si...

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Bibliographic Details
Published inTectonophysics Vol. 890; p. 230497
Main Authors An, Mengke, Yin, Zhen-Yu, Zhang, Fengshou, Huang, Rui, Elsworth, Derek
Format Journal Article
LanguageEnglish
Published Elsevier B.V 07.11.2024
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